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Shi Maochong, Chen Chunhua, Huang Fang, Ye Anle. Characteristics of tidal current and residual currentin the Qiongzhou Straits in period between end of winter and beginning of spring[J]. Haiyang Xuebao, 1998, 20(1): 1-10.
Citation: Shi Maochong, Chen Chunhua, Huang Fang, Ye Anle. Characteristics of tidal current and residual currentin the Qiongzhou Straits in period between end of winter and beginning of spring[J]. Haiyang Xuebao, 1998, 20(1): 1-10.

Characteristics of tidal current and residual currentin the Qiongzhou Straits in period between end of winter and beginning of spring

  • Received Date: 1997-02-01
  • Rev Recd Date: 1997-07-15
  • From Februarg.26 to March 6,1995, the currents on 15 stations between Xinghai and Sitang are measured.The characteristics of the currents are as follows:The speeds of flood current are larger than ebb current.The maximum flood speed is 172 cm/s,the maximum ebb speed is 142 cm/s;the speed of mean residual current on north 6 stations is 18.4 cm/s.The speed of mean residual current on middle 3 stations of the straits is 18.3 cm/s.The speed of mean residual current on south 6 stations is 10.2 cm/s.The directions of residual currents are in range W-S on northern and middle stationss,and in range N-NE on southern stations, because of the influence of the topography.This paper has used a model to calculate the tidal currents in the straits.The sum of the water amount passing through the west section (Dengloujiao-Yubaojiao) is 4.73×1010m3 (by ebb current).and is 4.29×1010m3 (by flood tide).The sum of the water amount passing through the east section (Dongying-Longtangzhen) is 5.22×1010m3 (by ebb current) and is 1.90×1010m3 (by flood tidal current).The net amounts are 0.43×1010m3 (west section) and 0.32×1010m3 (east section).The direction of the net transportation points toward west.
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  • 曹德明,方国洪.北部湾潮汐和潮流的数值模拟.海洋与湖沼,1990,21(2):105-120
    Ye Anle,Robinson L S.Tidal dynamics in the South China Sea.Geophy.J.R.Astro.Soc.,1983,72,691-707
    柯佩辉.琼海海峡的海流和水交换的初步分析.热带海洋,1983,2(1):25-31
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